Scientists to drill into a crack in the edge of the world

July 18th, 2008 - 1:48 pm ICT by ANI  

Wellington, July 18 (ANI): An international consortium of scientists is preparing to drill into a crack in the edge of the world the South Islands Alpine Fault in New Zealand.

The researchers want to drill over 5km deep in the Mt. Cook National Park, west of Lilybank, in a cutting-edge experiment which will give a look at changes within the fault, which is expected to eventually destroy large areas of the South Island in a magnitude 8 quake.

By drilling a hole into a fault in the Earths mid-crust, the scientists will get a close look at changes in the underlying rock, and whether the fault is being lubricated by fluids under huge pressures or even talc associated with layers of serpentinite under the Southern Alps.

Average slip rates in the faults central region are about 30mm a year, very fast by global standards.

We can take advantage of a rare window into the physical character of the seismologically expressed brittle-ductile transition zone in a fault that is active today and which can be geophysically monitored in the coming decades, said the researchers in the International Continental Scientific Drilling Programme (ICDP).

Victoria University geophysicist and Earthquake Commission fellow in seismic studies, John Townend, proposed the ambitious, technically challenging drillhole.

A drillhole allows the measurement of stress, the pressure of fluids, the temperature, the heat flow, the chemistry of the fluids, the rocks and any gases in the fault zone.

Establishment of a fault-hosted observatory will allow continuous observation of a fault that is late in its earthquake cycle, he said.

The Alpine Fault is thought to fail in magnitude 8 quakes at intervals between 100 and 400 years, the most recent being 291 years ago, in 1717.

The 1717 quake appears to have involved a rupture along nearly 400km of the southern two thirds of the fault, and some researchers have said a similar earthquake could happen at any time, as the interval since 1717 is longer than between the earlier events.

According to Dr Townend, the drillhole also offers the exciting possibility of recording data before and during a future large earthquake.

Also, samples from the drilling will be able to be compared with young rock now on the surface, about 7km above the fault, which some scientists believe has been particularly brittle under extreme pressures when it was underground, and to have be exposed to big pressure changes exerted by fluid deep in the earth. (ANI)

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